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Home›Spatial analysis›Conditional Geostatistical Simulation
Regression modelGeostatistics

Conditional Geostatistical Simulation

Sequential Gaussian Simulation (Conditional Simulation) · Also known as: Sequential Gaussian Simulation, SGS, Stochastic Simulation, Koşullu Simülasyon

Conditional Geostatistical Simulation — most commonly implemented as Sequential Gaussian Simulation (SGS) — generates multiple stochastic realizations of a spatial random field that are each consistent with observed sample data and with a fitted variogram model. Unlike kriging, which produces a single smoothed estimate, SGS reproduces the full spatial variability of the phenomenon. It is widely used by geoscientists, mining engineers, petroleum engineers, and environmental scientists who need to propagate spatial uncertainty through downstream models.

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Conditional Geostatistical Simulation
CokrigingUniversal Kriging

When to use it

Use conditional simulation when you need to quantify spatial uncertainty rather than obtain a single best estimate. It is appropriate when the variogram can be reliably fitted to the data and when a multi-Gaussian assumption for the transformed variable is defensible. Simulation is especially valuable for non-linear transfer functions — ore reserves, contaminant plume volumes, flow simulations — where the smooth kriging estimate would bias results. If a single optimal estimate suffices, kriging is simpler. If data are too sparse to fit a reliable variogram, simulation results may be unreliable.

Strengths & limitations

Strengths
  • Reproduces the full spatial variability described by the variogram, avoiding the smoothing artifact inherent in kriging.
  • Provides multiple equiprobable realizations that enable rigorous Monte Carlo uncertainty propagation through any downstream model.
  • Honors hard conditioning data exactly at sample locations by construction.
  • Flexible enough to incorporate secondary variables (co-simulation) or inequality constraints through appropriate CCDF transformations.
Limitations
  • Computationally intensive: generating hundreds of realizations over fine grids can be demanding, though modern implementations (GSLIB, SGeMS, gstat) are optimized.
  • Requires a reliable variogram model; poor variogram fitting leads to realizations with incorrect spatial continuity.
  • The multi-Gaussian assumption may be violated for data with strong spatial connectivity of extreme values, such as channelized facies.
  • Post-processing many realizations demands additional infrastructure for summarizing uncertainty (P10/P50/P90, probability maps).

Frequently asked

How many realizations do I need?

The required number depends on the stability of the statistic of interest. For simple spatial averages, 50–100 realizations often suffice. For tail quantiles, connectivity metrics, or flow simulations, 200–500 or more may be needed. A practical approach is to increase L until the empirical distribution of the target statistic stabilizes.

Does SGS always reproduce the variogram?

Each individual realization is a sample from the correct spatial distribution and will approximately reproduce the variogram on average across realizations, but any single realization will show statistical fluctuations around the model variogram. Averaging many realizations (the E-type) will reproduce the variogram mean but underestimate variance — it is not itself a valid realization.

What is the difference between conditional and unconditional simulation?

Unconditional simulation generates spatially correlated random fields consistent with a variogram model but ignores any observed data. Conditional simulation additionally constrains each realization to match the measured values at sample locations. For practical resource and risk assessment, conditional simulation is almost always the appropriate choice when data are available.

Sources

  1. Goovaerts, P. (1997). Geostatistics for Natural Resources Evaluation. Oxford University Press. ISBN: 978-0-19-511538-3

How to cite this page

ScholarGate. (2026, June 2). Sequential Gaussian Simulation (Conditional Simulation). ScholarGate. https://scholargate.app/en/spatial-analysis/conditional-simulation

Related methods

CokrigingUniversal Kriging

Which method?

Set this method beside its closest kin and read them side by side — the library lays the books on the table; the choice is yours.

  • CokrigingSpatial analysis↔ compare
  • Universal KrigingSpatial analysis↔ compare
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Similar methods

Spatial Monte Carlo SimulationKrigingBayesian KrigingBayesian Ordinary KrigingOrdinary KrigingGlobal Ordinary KrigingCokrigingCo-kriging

Related reference concepts

Gibbs SamplingGibbs Sampling (Statistical Computing)Monte Carlo MethodsGaussian Process ModelsStatistical Simulation Methods: GeneralVariance Reduction Techniques

Spotted an issue on this page? Report or suggest a fix →

ScholarGate — Conditional Geostatistical Simulation (Sequential Gaussian Simulation (Conditional Simulation)). Retrieved 2026-07-20 from https://scholargate.app/en/spatial-analysis/conditional-simulation · Dataset: https://doi.org/10.5281/zenodo.20539026
Quick facts
Originator
Pierre Goovaerts; geostatistics tradition
Year
1997
Type
Stochastic spatial simulation
Subfamily
Geostatistics
Output
Multiple equally probable realizations of a spatial field
Related methods
CokrigingUniversal Kriging
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